High Rate Determinations of Dimethyl Sulfide and Sulfur Dioxide during Rain In Cumulus over the Ocean (RICO)

海洋上空积云降雨​​期间二甲硫醚和二氧化硫的高速测定 (RICO)

• 批准号: 0342138
• 负责人: Alan Bandy
• 金额: $ 28.93万
• 依托单位: Drexel University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2004
• 资助国家: 美国
• 起止时间: 2004-03-01 至 2007-02-28
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0342138&HistoricalAwards=false
• 关键词: Rate; Determinations; Dimethyl; Sulfide; Sulfur

Dimethyl sulfide (DMS) is produced in and released from the ocean but decays slowly in the atmosphere (primarily by oxidation to sulfur dioxide). It is also nearly insoluble in cloud water, so it provides a good tracer for boundary-layer air in oceanic clouds. In contrast, sulfur dioxide dissolves readily in cloud water so the decay of sulfur dioxide in clouds can provide a measure of cloud lifetime. In this study, the investigators will measure DMS and sulfur dioxide as part of the broader "Rain in Cumulus over the Ocean" (RICO) experiment, a multi-investigator study of warm-rain formation and the characteristics of trade-wind Cumuli. They will use DMS to track boundary-layer air as it moves into clouds and mixes with DMS-free air from above, and they will use sulfur dioxide concentration as an indicator of cloud lifetime. A primary objective of RICO is to understand the rate of warm-rain formation, so the measurement of cloud age will be a valuable contribution to that broader study. The DMS measurements will also indicate how much dilution of cloud parcels occurs by mixing with drier air from above. In addition, the investigators will examine the oxidation processes in and near clouds and the roles of such processes in the formation of new particles or the growth of existing particles. If successful, these measurement techniques can have broad applications in future studies of clouds. Other contributions to future capabilities include the training of a new investigator in this area of research and a contribution to the planned RICO graduate-student seminar that will expose graduate students to many of the leaders in this field of research.

二甲基硫（DMS）在海洋中产生和释放，但在大气中缓慢衰减（主要通过氧化为二氧化硫）。它也几乎不溶于云水，因此它为海洋云中的边界层空气提供了一个很好的示踪剂。相比之下，二氧化硫很容易溶解在云水中，因此二氧化硫在云中的衰减可以提供云寿命的测量。在这项研究中，研究人员将测量DMS和二氧化硫，作为更广泛的“海洋积云降雨”（RICO）实验的一部分，这是一项关于暖雨形成和信风积云特征的多研究者研究。他们将使用DMS来跟踪边界层空气，因为它移动到云中，并与来自上方的无DMS空气混合，他们将使用二氧化硫浓度作为云寿命的指标。RICO的主要目标是了解暖雨形成的速度，因此云年龄的测量将对更广泛的研究做出有价值的贡献。DMS的测量还将表明云层与来自上方的干燥空气混合后会发生多少稀释。此外，研究人员还将研究云中和附近的氧化过程，以及这些过程在形成新粒子或现有粒子生长中的作用。如果成功的话，这些测量技术可以在未来的云研究中得到广泛的应用。对未来能力的其他贡献包括在这一研究领域培训一名新的调查员，并对计划中的RICO研究生研讨会作出贡献，该研讨会将使研究生接触这一研究领域的许多领导人。